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of the metamorphic rock will be the set of all P-T situations professional by a rock all through its metamorphic heritage (Figure 1).

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Utilizing zoning information to reconstruct the part of the P-T route experienced through the zoned mineral just isn't easy, but some typical areas of the connection of zoning to P-T path may well effortlessly be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims file growth zoning that signifies the change through the reduce-T ailments at which the garnet core grew to the upper-T circumstances at which the garnet rim grew (i.e., prograde metamorphism involving raising temperature and stress). Mn is preferentially partitioned into garnet relative to most other prevalent minerals, so Mn is sequestered in early-fashioned garnet, depleting the nearby natural environment in the escalating garnet in Mn. (b) Minerals that present important factor advancement zoning almost certainly didn't expertise pretty large metamorphic temperatures. At superior temperature (> seven hundred C) and ample duration, zoning can be homogenized as intracrystalline diffusion gets to be 台北硬碟救援 more practical at getting rid of compositional variation.

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